The following sections of this BookRags Literature Study Guide is offprint from Gale's For Students Series: Presenting Analysis, Context, and Criticism on Commonly Studied Works: Introduction, Author Biography, Plot Summary, Characters, Themes, Style, Historical Context, Critical Overview, Criticism and Critical Essays, Media Adaptations, Topics for Further Study, Compare & Contrast, What Do I Read Next?, For Further Study, and Sources.
(c)1998-2002; (c)2002 by Gale. Gale is an imprint of The Gale Group, Inc., a division of Thomson Learning, Inc. Gale and Design and Thomson Learning are trademarks used herein under license.
The following sections, if they exist, are offprint from Beacham's Encyclopedia of Popular Fiction: "Social Concerns", "Thematic Overview", "Techniques", "Literary Precedents", "Key Questions", "Related Titles", "Adaptations", "Related Web Sites". (c)1994-2005, by Walton Beacham.
The following sections, if they exist, are offprint from Beacham's Guide to Literature for Young Adults: "About the Author", "Overview", "Setting", "Literary Qualities", "Social Sensitivity", "Topics for Discussion", "Ideas for Reports and Papers". (c)1994-2005, by Walton Beacham.
All other sections in this Literature Study Guide are owned and copyrighted by BookRags, Inc.
Natural zones below the surface that yield water in sufficient quantities to be economically important for industrial, agricultural, or domestic purposes. Aquifers can occur in a variety of geologic materials, ranging from glacial-deposited outwash to sedimentary beds of limestone and sandstone, and fractured zones in dense igneous rocks. Composition and characteristics are almost infinite in their variety.
Aquifers can be confined or unconfined. Unconfined aquifers are those where direct contact can be made with the atmosphere, while confined aquifers are separated from the atmosphere by impermeable materials. Confined aquifers are also artesian aquifers. Though originally artesian was a term applied to water in an aquifer under sufficient pressure to produce flowing wells, the term is now generally applied to all confined situations.